Abstract
The structure of the lithosphere is key to reconciling the dynamic topography predicted by mantle convection models with residual topography derived from observations, suggest analyses of both models and data.
The structure of the lithosphere is key to reconciling the dynamic topography predicted by mantle convection models with residual topography derived from observations, suggest analyses of both models and data.
Publication Details
Flament, N. (2019). The deep roots of Earth’s surface. Nature Geoscience, 12 787-788.